Ehsan Zarrinabadi, David A. Lobb, Masoud Goharrokhi, Eric Enanga, Purbasha Mistry, Pascal Badiou, Irena F. Creed
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引用次数: 0
Abstract
Depressional wetlands in the Canadian Prairies are experiencing degradation due to intensive agricultural practices in adjacent upland areas. Depressional wetlands within cropland are particularly affected, as increased sedimentation and runoff elevate nutrient levels within these ecosystems. This study assessed soil organic carbon (SOC) and soil particulate phosphorus (SPP) stocks, fluxes, and balances within the contributing catchment area to depressional wetlands. Catchment-scale sediment tracing using 137Cs and budgeting methods was employed to examine the interactions between soil degradation, sediment movement, and nutrient redistribution. Analysis of 165 soil/sediment cores from eight wetland catchments revealed spatial heterogeneity in SOC and SPP stocks across upper-, middle-, and lower-slope and depression topographical sequences. SOC levels ranged from 6.9 to 104.1 kg m−2, while SPP varied from 0.06 to 1.9 kg m−2 within soil depth profile. Riparian areas at slope bottoms emerged as key accumulation sites for sediment, SOC, and SPP, underscoring their role as natural filters that intercept sediment and nutrients before they reach wetlands. These findings highlight the vulnerability of Canadian Prairie depressional wetlands to sediment and nutrient loading, emphasizing the need for soil erosion control strategies—such as the conservation of riparian buffers—to mitigate the adverse effects of agricultural activities on these vital ecosystems.
由于邻近高地地区的集约化农业实践,加拿大大草原的洼地湿地正在退化。农田内的洼地湿地受到的影响尤其严重,因为泥沙和径流的增加提高了这些生态系统内的营养水平。本研究评估了洼地湿地贡献流域的土壤有机碳(SOC)和土壤颗粒磷(SPP)储量、通量和平衡。采用137Cs法和预算法进行流域尺度泥沙示踪,研究了土壤退化、泥沙运动和养分再分配之间的相互作用。通过对8个湿地集水区165个土壤/沉积物岩心的分析,揭示了上、中、下坡和洼地地形序列中有机碳和SPP储量的空间异质性。土壤有机碳含量变化范围为6.9 ~ 104.1 kg m−2,SPP变化范围为0.06 ~ 1.9 kg m−2。斜坡底部的河岸区是沉积物、有机碳和SPP的主要聚集点,强调了它们作为天然过滤器的作用,在沉积物和营养物质到达湿地之前就将其拦截。这些发现强调了加拿大草原洼地湿地对沉积物和养分负荷的脆弱性,强调了土壤侵蚀控制策略的必要性,例如保护河岸缓冲带,以减轻农业活动对这些重要生态系统的不利影响。